Background:
Diatoms
are single celled organisms that have shells composed of silica. These
incredibly diverse tiny organisms can be found in both freshwater and marine
ecosystems. They are often studied as important indicators of past ecological
conditions, because when the diatom dies, the silica shells remain in the
sediment. Because they remain in
the sediment for long periods of time, the composition of diatoms found at a
specific location in a soil core can tell researchers what conditions were like
when that layer was deposited. Diatoms can indicate water salinity,
temperature, and pH, as well as show nutrient and pollution levels in a system.
For example, imagine a system that experienced no pollution until humans
developed the surrounding area. The diatom composition before and after human
development would differ. You would expect to see more pollution tolerant
diatoms in the soil after development, and fewer pollution sensitive diatom
species.
Extracting a Core
Sediment core extraction required several
pieces of equipment. Two boats were used to navigate the body of water (lake)
in order to find a desired location for an extraction. Once a desired location
was found, the boat remained stationary for a minute to ensure no sediment
agitation occurred before taking a sample. Then, the core tube was slowly
lowered into the water and forcefully pushed into the sediment, reaching a
desired depth. The extraction of the core was performed by careful lifting of
the sediment core tube, followed by a quick placement of a rubber stopper at
the end of the tube. Finally, both ends of the core tube were plugged and taped
to insure preservation of the sample. While, performing a sediment core
extraction, it was observed that the bottom of the core was fairly dark due to
anoxic conditions that are associated with deeper sediment layers. The top
however, observed a brown-dark greenish color, indicating higher levels of
oxygen. While extruding the sediment core, the pH of water was tested using a
pH meter, which indicated a fairly neutral and acceptable value within the
range of 6.5 to 8.
Removing the Bottom Stopper and Inserting Plunger |
Creating Samples
Samples from a sediment core are important in studying the history of a desired body of water. They are great indicator of historical biodiversity which can be used to recreate past environments conditions. This information can be compared to the present biodiversity and further analyzed in order to grasp a better understanding of the changing environmental conditions such as the pH, as well as nutrient and pollution concentrations within the body of water.
Samples from a sediment core are important in studying the history of a desired body of water. They are great indicator of historical biodiversity which can be used to recreate past environments conditions. This information can be compared to the present biodiversity and further analyzed in order to grasp a better understanding of the changing environmental conditions such as the pH, as well as nutrient and pollution concentrations within the body of water.
Extruding the Soil Core |
In
order to create samples from the extruded core, whirlpac bags were obtained and
labeled to ensure accurate tracking of samples. Then, the water layer present
inside the sediment core tube was expelled using a plunger- like tool that
pushed the sediment from the bottom to the top. A specially designed tray was
fitted on top of the sediment core which was used to concentrate the sediment
samples into 1 cm intervals. The intervals were collected (by scraping the top)
and stored inside designated whirlpac bags. All of the samples collected were
then further analyzed by preparing microscopic slides in order to observe
diatom biodiversity.
This Plate Helps Measure Out 1cm of soil |
Samples are Scraped into Whirlpak Bags for Sampling |
Preparing Slides
To
analyze the diatoms in the sample, they must be spread out onto microscope
slides. The first step in slide preparation is to remove as much of the organic
matter and soil from your samples. This can be done by boiling a small about of
sample in nitric acid, to break down organic compounds. After the samples are
boiled, they are rinsed with water several times to remove traces of acid. The
finished diatom mixture is cloudy and will need to be diluted farther before it
can be made into slides. It is recommended that you make three separate
dilutions of each sample while making slides.
Boiling Samples to Purify Them |
A Purified Sample: Ready for Dilution and Slides |
The
slides themselves are made by placing the sample onto a clean cover slip. The sample should cover the entire
cover slip and form a mound in the middle. These will need to sit for at least
twenty-four hours, as they dry.
Once dry, the cover slips can be permanently mounted to a clean
microscope slide. Attaching the
cover slips permanently allows researchers to preserve samples for later
analysis.
Alison Demonstrates How to Correctly Make A Slide |
Make sure to get a mound of water in the middle of your cover slip. It shouldn't spill onto other cover slips. |
No comments:
Post a Comment